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Seasons and Atmosphere Observations Globe Lamp Ann’s Book. Astronomy Activity 10 (pg 83) Reason for the seasons What do you already know about the Earth? How do you think Earth formed? What is Earth’s position in the solar system? How does planet Earth compare to the other planets in the solar system? How close is Earth to other planets? How do Earth and other planets move through the galaxy? Probe to get them towards Revolution. In one day are you always the same distance from the sun? How do we have day and night? Probe to get them towards Rotation. Revolution Motion of a body along a path around some point in space. Earth’s orbit is elliptical Earth’s distance from the sun varies Perihelion Earth is closest to the sun 147 million km away Occurs on January 3rd Aphelion Earth is farthest from the sun 152 million km away Occurs on July 4th Rotation The turning or spinning of a body on its axis Causes day and night Two kinds of measurement Mean Solar Day – time interval from one noon to the next (24 hours) Sidereal Day – time it takes for Earth to make one complete rotation (360’) with respect to a star other than the sun (23 hours, 56 minutes, 4 seconds) Put out a globe for students to look at. What do you notice about the shape or the orientation of Earth? Probe them to get to tilt Have you ever wondered why the Earth is tilted instead of just perpendicular with its plane of orbit? What is gravity? How is matter measured? Now relate rotation and revolution back to earth’s tilted axis and how the axis causes seasons. Activity- Simulation – gather observations (discuss) Get them to seasons from the tilt. Seasons are caused by the tilting of the earth on its axis (23.5°) When the Earth is tilted towards the Sun – warmer seasons When the Earth is tilted away from the Sun – cooler seasons Meteorology Activity 6 (Pg. 59) Heating of thermometers tilted at different angles. What type of weather do you experience during the four seasons? What is the study of weather? What is another term that you associate with weather? Where does weather occur? What is our air made of? *lead them to water vapor is made in the atmosphere also = clouds/air masses Is the air the same at different temperatures? FOLDABLE Layers of the atmosphere Whats the difference between the air around you on the ground and the air outside of an airplane. Mountain Range picture: Why is their snow on top of the mountains but not at the base? The study of weather, climate, and atmospheric processes Weather is constantly changing and it refers to the state of the atmosphere at any given time and place Climate is based on observations of weather that have been collected over many years to help describe a place or region Main Components Nitrogen – 78% Oxygen – 21% CO2 < 1% Argon < 1% Air pollution is airborne particles and gases that occur in concentrations large enough to endanger the health of organisms Primary Pollution: emitted directly from identifiable sources Secondary Pollutions: not emitted directly into air (agriculture) Water vapor - source of all clouds and precipitation. The three states of matter solid, liquid, and gas (plasma is the fourth) Precipitation Condensation Evaporation Precipitation is any form of water that falls from a cloud. © When it comes to understanding atmospheric processes, water vapor is the most important gas in the atmosphere © amount of water vapor in air. © © © Ratio of the air’s actual water-vapor content compared with the amount of water vapor air can hold at that temperature and pressure. Lowering air temperature causes an increase in relative humidity Raising air temperature causes a decrease in relative humidity ⬜ ⬜ ⬜ ⬜ Instrument: Hygrometer Psychrometer : a type of hygrometer consisting of two identical thermometers mounted side by side Dry bulb: give the present air temperature Wet bulb: has thin wet wick tied around the end Dew point is the temperature to which a parcel of air would need to be cooled to reach saturation. Clouds are classified on the basis of their form and height. Cirrus (cirrus = curl of hair) high, white, and thin Cumulus (cumulus = a pile) rounded individual cloud masses that have a flat base and the appearance of rising domes or towers Stratus (stratus = a layer) best described as sheets or layers that cover much or all of the sky Clouds form when air is cooled to its dew point For precipitation to form, cloud droplets must grow in volume by roughly one million times. The type of precipitation that reaches Earth’s surface depends on the temperature profile in the lower few km of the atmosphere © Rain: drops of water that fall from a cloud and have a diameter of at least 0.5 mm © © Snow: light, fluffy, sixsided ice crystals © Sleet: fall of small particles of clear to translucent ice © Glaze: when raindrops become supercooled as they fall through subfreezing air and turns to ice when they impact objects © Hail: form of solid precipitation which consists of balls of irregular lumps of ice produced in cumulonimbus clouds ⬜ A cloud with its base at or very near the ground. The atmosphere rapidly thins as you travel away from Earth until there are too few gas molecules to detect. Pressure Changes Temperature Changes As you increase in altitude, or travel away from Earth, pressure decreases As you increase in altitude in the Troposphere the temperature decreases. Density Changes The Troposphere - the bottom layer Temperature decreases with an increase in altitude. Where weather occurs Tropopause: boundary of the troposphere The Stratosphere Above the troposphere Temperature remains constant, then gradually starts to increase Contains the ozone layer Stratopause: boundary of the stratosphere The Mesosphere Above the stratosphere Temperature decreases with height Mesopause: boundary of the mesosphere The Thermosphere: Upper layer of the atmosphere Temperature increase with height Auroras occur here Fades into space How does the temperature move about in the layers of the atmosphere? Move them towards convection, conduction, and radiation. Heat: the energy transferred from one object to another because of a direct difference in their temperature Temperature: measure of the amount of heat Heat transfer from HOT to COLD objects Conduction The transfer of heat through matter by molecular activity Transfer by touching Convection The transfer of heat by a mass movement or circulation within a substance Radiation Travels out in all directions Solar energy reaches earth by radiation Reflection occurs when light bounces off an object. 30 % of all radiation is reflected back to space Scattering produces a larger number of rays that travel in many directions. Absorption: 50 % of the solar energy that strikes the top of the atmosphere reaches the Earth’s surface 20% is absorbed in the clouds 30% is reflected back to space Ozone is a form of oxygen that combines three oxygen atoms into each molecule (O3) • Ozone filters and absorbs harmful UV radiation by the sun • Heating of Land and Water Activity Lead them back into temperatures varying on LAND! Discuss from activity Observations Follow- up question: What other factors affect the temperature of an area on land? Factors: Heating of land Heating of water Altitude Geographic position Cloud cover Ocean currents Land heats and cools more rapidly and to higher temperatures than water Water – heats up longer and will retain the heat longer Albedo the fraction of total radiation that is reflected by any surface. Daylight Cloud Cover Clouds reflect solar radiation back to space Temperatures are lower than on a clear day Nighttime Cloud Cover Clouds absorb radiation from land and reradiates some of it back to Earth Temperatures are higher than on a clear night Isotherms - lines on a weather map that connect points that have the same temperatures